“…Sensors designed to capture primary and/or induced precursory signals will measure a high number of parameters, combined with an array of seismographs detecting changes in background seismicity (Sammis and Sornette, 2002;Shebalin et al, 2006;Peresan, 2018) to recognize foreshock activity (Papadopoulos et al, 2018). Other sensors are destined to point out subtle changes of the physical parameters (e.g., temperature, mass-flux, and gas flow rate fluctuations) and composition of fluids (dissolved ions, dissolved gases, soil gas, CO 2 , CH 4 , He, H, radon, and thoron) (Zoran et al, 2012;Oh and Kim, 2015;Martinelli, 2020) circulating in the crust (e.g., Tsunogai and Wakita, 1995;Claesson et al, 2004;Hartman et al, 2005;Fu and Lee, 2018;Martinelli and Dadomo, 2018). Ground deformation and other space-monitorable atmospheric and ionospheric signals (e.g., Sgrigna et al, 2007;Hayakawa et al, 2018;Tramutoli et al, 2018a) might be considered to complete the ground-based monitoring system.…”